1887

Abstract

The tomographic inversion of the attenuation of reflected arrivals, through the frequency shift method is tested on a synthetic case and successively applied on the real data set acquired offshore Western Svalbard within the Hydratech EU project. The spatial variation (vertical and lateral ) of Qp are in agreement with Vp variations and with the presence of gas-hydrate and free-gas within the sediments.

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/content/papers/10.3997/2214-4609.201405173
2005-06-13
2020-10-25
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201405173
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